Increases in Ca/Mg ratios caused the increases in the mobile fractions of Cr and Ni in serpentinite-derived soils in humid Asia
Serpentinite-derived soils are characterized by low Ca/Mg ratio and abnormally high Cr and Ni concentrations due to the geogenic sources. The breakdown of parent materials during pedogenesis may lead to the changes in both Ca/Mg ratios and fractions of Cr and Ni. This study hypothesized that total C...
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Elsevier
2022
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| Truy cập trực tuyến: | https://www.sciencedirect.com/science/article/abs/pii/S0341816222004040?via%3Dihub https://dlib.phenikaa-uni.edu.vn/handle/PNK/5980 https://doi.org/10.1016/j.catena.2022.106418 |
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oai:localhost:PNK-59802022-08-17T05:54:51Z Increases in Ca/Mg ratios caused the increases in the mobile fractions of Cr and Ni in serpentinite-derived soils in humid Asia C.Y.Yang D.Q.Nguyen H.T.T.Ngo Ca/Mg ratios Potentially mobile fractions Serpentinite-derived soils are characterized by low Ca/Mg ratio and abnormally high Cr and Ni concentrations due to the geogenic sources. The breakdown of parent materials during pedogenesis may lead to the changes in both Ca/Mg ratios and fractions of Cr and Ni. This study hypothesized that total Ca/Mg (Cat/Mgt) and exchangeable Ca/Mg (Cae/Mge) ratios increase with soil development, associated with the increases in potentially mobile fractions (PMFs) of Cr and Ni. Thirty-five soil horizon samples of eight pedons from Japan, Taiwan, Philippines, and Vietnam were collected, and the exchangeable concentrations of Ca and Mg were measured. 2022-07-13T02:00:13Z 2022-07-13T02:00:13Z 2022 Bài trích https://www.sciencedirect.com/science/article/abs/pii/S0341816222004040?via%3Dihub https://dlib.phenikaa-uni.edu.vn/handle/PNK/5980 https://doi.org/10.1016/j.catena.2022.106418 en Elsevier |
| institution |
Digital Phenikaa |
| collection |
Digital Phenikaa |
| language |
English |
| topic |
Ca/Mg ratios Potentially mobile fractions |
| spellingShingle |
Ca/Mg ratios Potentially mobile fractions C.Y.Yang D.Q.Nguyen H.T.T.Ngo Increases in Ca/Mg ratios caused the increases in the mobile fractions of Cr and Ni in serpentinite-derived soils in humid Asia |
| description |
Serpentinite-derived soils are characterized by low Ca/Mg ratio and abnormally high Cr and Ni concentrations due to the geogenic sources. The breakdown of parent materials during pedogenesis may lead to the changes in both Ca/Mg ratios and fractions of Cr and Ni. This study hypothesized that total Ca/Mg (Cat/Mgt) and exchangeable Ca/Mg (Cae/Mge) ratios increase with soil development, associated with the increases in potentially mobile fractions (PMFs) of Cr and Ni. Thirty-five soil horizon samples of eight pedons from Japan, Taiwan, Philippines, and Vietnam were collected, and the exchangeable concentrations of Ca and Mg were measured. |
| format |
Bài trích |
| author |
C.Y.Yang D.Q.Nguyen H.T.T.Ngo |
| author_facet |
C.Y.Yang D.Q.Nguyen H.T.T.Ngo |
| author_sort |
C.Y.Yang |
| title |
Increases in Ca/Mg ratios caused the increases in the mobile fractions of Cr and Ni in serpentinite-derived soils in humid Asia |
| title_short |
Increases in Ca/Mg ratios caused the increases in the mobile fractions of Cr and Ni in serpentinite-derived soils in humid Asia |
| title_full |
Increases in Ca/Mg ratios caused the increases in the mobile fractions of Cr and Ni in serpentinite-derived soils in humid Asia |
| title_fullStr |
Increases in Ca/Mg ratios caused the increases in the mobile fractions of Cr and Ni in serpentinite-derived soils in humid Asia |
| title_full_unstemmed |
Increases in Ca/Mg ratios caused the increases in the mobile fractions of Cr and Ni in serpentinite-derived soils in humid Asia |
| title_sort |
increases in ca/mg ratios caused the increases in the mobile fractions of cr and ni in serpentinite-derived soils in humid asia |
| publisher |
Elsevier |
| publishDate |
2022 |
| url |
https://www.sciencedirect.com/science/article/abs/pii/S0341816222004040?via%3Dihub https://dlib.phenikaa-uni.edu.vn/handle/PNK/5980 https://doi.org/10.1016/j.catena.2022.106418 |
| _version_ |
1751856291450454016 |
| score |
8.881002 |